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Mesoproterozoic Era

geochronology
Also known as: Middle Proterozoic Era

Quick Summary

The Mesoproterozoic Era is a division of geologic time within the Proterozoic Eon, spanning from approximately 1.6 billion to 1 billion years ago. This era is part of the Precambrian, the longest eon in Earth's history. During the Mesoproterozoic, significant geological events included the assembly and breakup of supercontinents, such as Rodinia.123

The Proterozoic Eon, in general, saw major changes in Earth's atmosphere and oceans, including the accumulation of oxygen due to photosynthesis. Rocks from this eon often contain valuable metallic ores like iron, gold, copper, uranium, and nickel. While Precambrian fossils are scarce, the Proterozoic is notable for containing traces of early life-forms, including bacteria, blue-green algae, and the first oxygen-dependent animals. The Mesoproterozoic Era is defined by isotopic age determinations and is a period of significant continental evolution and plate movement.245

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